Shear partitioning in the eastern Nankai Trough: evidence from submersible dives
Shear partitioning in the eastern Nankai Trough: evidence from submersible dives
复制标题
南海海槽东部的剪切分区：潜水器潜水的证据
DOI：
10.1016/0012-821x(94)90136-8
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发表时间：
1994
影响因子：
5.3
通讯作者：
Kyoko Kobayashi
中科院分区：
文献类型：
--
作者：
X. Pichon;S. Lallemant;M. Fournier;J. Cadet;Kyoko Kobayashi
在南开海槽最东端的楔形区域潜水，证明了与俯冲带平行的左旋走滑系统的存在。这个系统随着海沟向北转向陆地而发展，对运动变得高度倾斜。尽管剪切分配在其他俯冲带中是众所周知的，但这里的过程具有继续向北进入陆地的特点。
Submersible dives over the wedge of the easternmost Nankai Trough demonstrate the existence of a left-lateral strike-slip system parallel to the subduction zone. This system develops as the trench, turning northward toward land, becomes highly oblique to the motion. Although shear partitioning is well known in other subduction zones, the process here has the peculiarity of continuing northward into land.